structural well balanced cross-portion benefits recommend that the overall fault slip of Hotan fault reaches ca. 358
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U-Pb and Hf isotopic within the east phase of Tiekelike tectonic belt: constrains around the timing 682
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insights to the style, timing and kinematics of deformation throughout this phase of the Western 78
the fault underwent sizeable action at late Oligocene to early Miocene, resulting in the 344
The structural Assessment with the seismic profile indicates that the growth strata began to produce 338
action of your Tiklik fault because mid- to late-Miocene is according to the unconformity among 451
Paleogene detachment layer and absorb substantial part of shortening during the segment (Liang et 72
reflections for the stratigraphic models inside the seismic profile. The structural and advancement strata model 156
Tiklik tiklik.com thrust zone and west on the Buya region associated with a footwall fault ramp just at north 443
earthquake: seismic dangers of an Energetic blind wedge thrust system for the Western Kunlun assortment 600
stage, the hanging wall of Tiklik fault slipped together the fault to uplift AFT samples within the study 421
early Miocene would end result to your unconformity involving N1 and E into the west of Buya, erosion of 449